Rock Identifier
Tumbled blue chalcedony or pale aquamarine-like quartz (Chalcedony (microcrystalline SiO₂), possibly blue quartz; visual identification is uncertain) — mineral
mineral

Tumbled blue chalcedony or pale aquamarine-like quartz

Chalcedony (microcrystalline SiO₂), possibly blue quartz; visual identification is uncertain

AI-generated identification · may be incorrect

Translucent blue-gray to colorless, vitreous/waxy luster, no visible cleavage, conchoidal fracture, and likely Mohs hardness about 6.5–7; rounded edges indicate tumbling or polishing.

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Physical properties

Translucent blue-gray to colorless, vitreous/waxy luster, no visible cleavage, conchoidal fracture, and likely Mohs hardness about 6.5–7; rounded edges indicate tumbling or polishing.

Formation & geological history

Quartz-rich silica formed from hydrothermal or groundwater fluids in cavities and fractures; chalcedony commonly formed during the Cenozoic, though its exact age cannot be determined visually.

Uses & applications

Used as a decorative tumbled stone, cabochon, carving material, and collector specimen; quality blue chalcedony may be used in jewelry.

Geological facts

The cloudy internal wisps and smooth polish are consistent with chalcedony, but the image alone cannot exclude glass or another quartz variety. Natural chalcedony commonly shows subtle fibrous translucency rather than distinct large crystals.

Field identification & locations

Test with a steel file or quartz point: genuine quartz should resist scratching; glass may show bubbles and scratches more readily. Common sources include Brazil, India, Madagascar, Turkey, and the United States.